Last century Greenland ice sheet surface mass balance projections from IPCC AR4 global models

Results from atmosphere-ocean general circulation models (AOGCM's) for the IPCC 4th Assessment Report are used to investigate surface mass balance (SMB) future projections of the Greenland ice sheet (GrIS). The most efficient models for the GrIS climate modeling are chosen by comparison between...

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Main Authors: Franco, Bruno, Fettweis, Xavier, Erpicum, Michel
Other Authors: Laboratoire de Climatologie et Topoclimatologie
Format: Conference Object
Language:English
Published: 2008
Subjects:
Online Access:https://orbi.uliege.be/handle/2268/59536
id ftorbi:oai:orbi.ulg.ac.be:2268/59536
record_format openpolar
spelling ftorbi:oai:orbi.ulg.ac.be:2268/59536 2024-10-20T14:09:03+00:00 Last century Greenland ice sheet surface mass balance projections from IPCC AR4 global models Franco, Bruno Fettweis, Xavier Erpicum, Michel Laboratoire de Climatologie et Topoclimatologie 2008-04 https://orbi.uliege.be/handle/2268/59536 en eng https://orbi.uliege.be/handle/2268/59536 info:hdl:2268/59536 European Geosciences Union General Assembly 2008, Vienna, Austria [AT], avril 2008 Greenland ice sheet surface mass balance IPCC AR4 models Physical chemical mathematical & earth Sciences Earth sciences & physical geography Physique chimie mathématiques & sciences de la terre Sciences de la terre & géographie physique conference poster not in proceedings http://purl.org/coar/resource_type/c_18co info:eu-repo/semantics/conferencePoster 2008 ftorbi 2024-09-27T07:01:41Z Results from atmosphere-ocean general circulation models (AOGCM's) for the IPCC 4th Assessment Report are used to investigate surface mass balance (SMB) future projections of the Greenland ice sheet (GrIS). The most efficient models for the GrIS climate modeling are chosen by comparison between the 1970-1999 outputs (averages and trends) from the 20C3M Experiment outputs, and the reanalyses (ECMWF, NCEP) as well as climatologies. The SMB is estimated from the summer temperature (from which is deduced the run-off) and annual snowfall from the well-adapted AOGCM's. It is validated with 1970-1999 results from the regional climate model MAR by interpolating the AOGCM's outputs on the MAR grid. However, large uncertainties remain in these SMB projections due to the simplified physic and coarse AOGCM's resolution. High resolution simulations made with the MAR model (which simulates explicitly the SMB by taking into account the surface feedbacks) forced at its boundaries by a GrIS well-adapted AOGCM could bring more precise brief replies. Conference Object Greenland Ice Sheet University of Liège: ORBi (Open Repository and Bibliography) Greenland
institution Open Polar
collection University of Liège: ORBi (Open Repository and Bibliography)
op_collection_id ftorbi
language English
topic Greenland
ice sheet surface mass balance
IPCC AR4 models
Physical
chemical
mathematical & earth Sciences
Earth sciences & physical geography
Physique
chimie
mathématiques & sciences de la terre
Sciences de la terre & géographie physique
spellingShingle Greenland
ice sheet surface mass balance
IPCC AR4 models
Physical
chemical
mathematical & earth Sciences
Earth sciences & physical geography
Physique
chimie
mathématiques & sciences de la terre
Sciences de la terre & géographie physique
Franco, Bruno
Fettweis, Xavier
Erpicum, Michel
Last century Greenland ice sheet surface mass balance projections from IPCC AR4 global models
topic_facet Greenland
ice sheet surface mass balance
IPCC AR4 models
Physical
chemical
mathematical & earth Sciences
Earth sciences & physical geography
Physique
chimie
mathématiques & sciences de la terre
Sciences de la terre & géographie physique
description Results from atmosphere-ocean general circulation models (AOGCM's) for the IPCC 4th Assessment Report are used to investigate surface mass balance (SMB) future projections of the Greenland ice sheet (GrIS). The most efficient models for the GrIS climate modeling are chosen by comparison between the 1970-1999 outputs (averages and trends) from the 20C3M Experiment outputs, and the reanalyses (ECMWF, NCEP) as well as climatologies. The SMB is estimated from the summer temperature (from which is deduced the run-off) and annual snowfall from the well-adapted AOGCM's. It is validated with 1970-1999 results from the regional climate model MAR by interpolating the AOGCM's outputs on the MAR grid. However, large uncertainties remain in these SMB projections due to the simplified physic and coarse AOGCM's resolution. High resolution simulations made with the MAR model (which simulates explicitly the SMB by taking into account the surface feedbacks) forced at its boundaries by a GrIS well-adapted AOGCM could bring more precise brief replies.
author2 Laboratoire de Climatologie et Topoclimatologie
format Conference Object
author Franco, Bruno
Fettweis, Xavier
Erpicum, Michel
author_facet Franco, Bruno
Fettweis, Xavier
Erpicum, Michel
author_sort Franco, Bruno
title Last century Greenland ice sheet surface mass balance projections from IPCC AR4 global models
title_short Last century Greenland ice sheet surface mass balance projections from IPCC AR4 global models
title_full Last century Greenland ice sheet surface mass balance projections from IPCC AR4 global models
title_fullStr Last century Greenland ice sheet surface mass balance projections from IPCC AR4 global models
title_full_unstemmed Last century Greenland ice sheet surface mass balance projections from IPCC AR4 global models
title_sort last century greenland ice sheet surface mass balance projections from ipcc ar4 global models
publishDate 2008
url https://orbi.uliege.be/handle/2268/59536
geographic Greenland
geographic_facet Greenland
genre Greenland
Ice Sheet
genre_facet Greenland
Ice Sheet
op_source European Geosciences Union General Assembly 2008, Vienna, Austria [AT], avril 2008
op_relation https://orbi.uliege.be/handle/2268/59536
info:hdl:2268/59536
_version_ 1813448465883070464